Exam 1 Terms Flashcards
sonar
SOund NAvagation Ranging
SCUBA
Self-Contained Underwater Breathing Apparatus
Ocean sizes (largest to smallest)
Pacific > Atlantic > Indian > Arctic
Main component of continental crust
granite
main component of oceanic crust
basalt
continental drift
hypothesis proposed by Alfred Wegener that continents had once been joined together in a supercontinent (Pangea)
plate tectonics
movement of tectonic plates on Earth’s surface
mid-ocean ridge system
continuous chain of submarine volcanic mountains that encircles the globe
faults
cracks in the earth’s crust
Mid-Atlantic Ridge
runs down center of atlantic ocean
East Pacific Rise
continuation of Mid-Atlantic Ridge in pacific ocean
trenches
deep depressions in the sea floor
sediment
loose material like sand and mud on bottom
magnetic anomalies
bands of rock on ocean floor alternating between normal and reversed magnetization
rift
crack created in earth’s crust by separating plates
sea-floor spreading
entire process by which the sea floor moves away from the mid-ocean ridges to create new sea floor
lithosphere
crust + uppermost layer of mantle. Forms tectonic plates
asthenosphere
plastic, upper part of the mantle which the tectonic plates float on.
subduction
downward movement of a plate into the mantle
subduction zone
trenches where subduction is happening
island arcs
volcanic island chains associated with trenches that follow the trenches’ curvature
shear boundry
fault line where plates slide past each other
continental margins
consist of gently sloping continental shelf, steeper continental slope, and gently sloping region called the continental rise
submarine canyons
formed by rivers and glaciers and then later submerged with rising sea level
shelf break
point where the slope gets abruptly steeper and the continental shelf ends
continental slope
begins at shelf break and descends down to deep-sea floor. Closest thing to exact edge of continent
deep-sea fan
accumulated sediment at the base of a submarine canyon. Forms continental rise
active margin
continental margin with lots of geological activity
passive margin
continental margin with little geological activity
abyssal plane
deep-sea floor
abyssal hills
hills on the sea floor
seamounts
submarine volcanoes
guyots
flattopped seamounts
chemical weathering
one source of many substances dissolved in seawater
hydrothermal vents
another source for chemicals dissolved in seawater
solutes
dissolved materials
salinity
total amount of salt dissolved in seawater
practical salinity units (psu)
expression used by oceanographers for salinity determined by conductivity measurements. Equivalent to ppt.
rule of constant proportions
percentage of major ions in seawater is always the same, even when salinity changes
temperature profile
graph showing temperature at different depths
water column
vertical shaft of water extending down from the surface
CTDs
Conductivity-Temperature-Depth meters